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Crustal structure and continent-ocean boundary along the Galicia continental margin (NW Iberia): insights from combined gravity and seismic interpretation ArchiMer
Druet, M.; Munoz-martin, A.; Granja-bruna, J. L.; Carbo-gorosabel, A.; Acosta, J.; Llanes, P.; Ercilla, G..
The magma‐poor rifted continental margin of Galicia has an extremely complex structure. Its formation involved several rifting episodes that occurred ultimately during the early Cretaceous near a ridge triple junction, which produced a change in the orientation of the main structures in its transition to the north Iberia margin. In addition, there is a superimposed partial tectonic inversion along its northwest and northern border which developed from the Late Cretaceous to at least Oligocene times. The present study integrates a large volume of new geophysical information (mainly marine gravity data and 2D seismic reflection profiles) to provide insights on the formation of this rift system and on the development of its later inversion. The combined...
Tipo: Text Palavras-chave: Rifted margin; Hyperextension; Tectonic inversion; Crustal domains; Structural domains; Gravity.
Ano: 2018 URL: https://archimer.ifremer.fr/doc/00438/54975/56420.pdf
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